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Studies on Real and Imaginary Part of Permeability for Sm-Dy Substituted Mg Ferrite

机译:SM-DY取代Mg铁素体渗透性的真实和虚构部分的研究

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The ferrite samples having composition Mg[(Sm)0.5(Dy)0.5]xFe2-xO4,in which x varies from 0.05 to 0.3 in steps of 0.05 have been prepared by using combustion method.X-ray diffraction analysis confirmed the formation of cubic spinel structure in addition of ortho-ferrite phase due to substitution of rare earth ions.The initial permeability and complex permeability of toroid samples are calculated by measuring the values of inductance and Q-factor.It is seen that initial permeability and real part of initial permeability increases with increase in Samarium(Sm)-Dysprosium(Dy)rare earth element in magnetium(Mg)up to x = 0.15 and thereafter it decreases.The composition Mg[(Sm)0.5(Dy)0.5]0.15Fe1.85O4 show low loss factor and initial permeability becomes higher as compared to other prepared rare earth content samples.
机译:具有组成Mg [(SM)0.5(Dy)0.5] XFE2-XO4的铁氧体样品,其中x在0.05的0.05〜0.3的过程中,通过使用燃烧方法制备.x射线衍射分析证实了立方体的形成 由于替代稀土离子而添加尖晶石结构。通过测量电感和Q-Factor的值来计算环形样品的初始渗透性和复杂渗透性。它看出了初始渗透性和初始的初始渗透性和实际部分 渗透性随着钐(Mg)的钐(Mg)稀土元素的增加而增加,高达X = 0.15,然后减少。组合物Mg [(Sm)0.5(Dy)0.5] 0.5Fe1.85O4显示 与其他制备的稀土含量样品相比,低损耗因子和初始渗透率变得更高。

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